Download Enders' Homöopathie für Kinder, 4. Auflage by Norbert Enders PDF

By Norbert Enders

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And Extension of Continental Crust WINCH profile (Fig. 26, 27, and 28) show abundant diffractions and the fault may extend vertically into the mantle where dipping reflections are apparently Rifts 1983. ) In Several deep seismic reflection traverse regions of important crustal In these data a variety of features extension can be observed. In profiles extension. , 1986). The reflection data there (Fig. S. several COCORPsurveys cross various parts of the Basin and Range province of Cenozoic to Recent normal faulting.

Kaufman, D. , 1982. C. Ando, S. Klemperer, the Geology, J. Oliver, ity. Akad. Nauk. I. Davydova, seismic crustal 1068-1084, 1965. Ein Beitrag Untergrundes, zur studies, Er{orschung Geologische des Rundschau, S. Kaufman,B. Czuchra,T. W. Isachsen, Adirondack-Appalachian crustal struc- 46, 17-26, 1957. , andK. Fuchs,Statistical evaluationof Soc. , 94, 1173-1184,1983. , M. Barazangi, S. Kaufman, and J. Oliver, The First Decadeof COCORP' 1974-1984, in Reflection Seismology' A Global Perspec- 32, 951-967, 1967.

26. Note Outer Isles Thrust (OIT) and Flannan Thrust (FT) as seen on MOIST (Figs. 24 and 25) and good reflections from Moho. NLB=North Lewis Basin, McBride across et the al, Great in Glen MB=Minch Basin. review). , 1983). and Extension of Continental Crust WINCH profile (Fig. 26, 27, and 28) show abundant diffractions and the fault may extend vertically into the mantle where dipping reflections are apparently Rifts 1983. ) In Several deep seismic reflection traverse regions of important crustal In these data a variety of features extension can be observed.

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